ISHIMSKY DISTRICT IN TERRITORIAL DISPUTES OF THE URALS AND SIBERIA OF THE EARLY 1920

2018 ◽  
Keyword(s):  
Territorial Disputes ◽  
The Urals

South Korea’s and Taiwan’s Territorial Disputes with Japan, 1990s to 2018

Asian Survey ◽  
2020 ◽  
Vol 60 (3) ◽  
pp. 583-606
Author(s):  
Christina Lai
Keyword(s):  
South Korea ◽  
Comparative Study ◽  
State Building ◽  
Territorial Disputes ◽  
Maritime Disputes ◽  
Constructivist Perspective ◽  
Senkaku Islands ◽  
Taiwanese Government

South Korea and Taiwan are former Japanese colonies that have undergone similar processes of state-building since WWII. But they have chosen different rhetorical frameworks in their maritime disputes with Japan. In South Korea, negotiating with Japan can be viewed as threatening the country’s independence and pride, whereas in the Taiwanese government, cooperation with Japan is considered mutually beneficial. Why have these two countries taken such divergent stances toward Japan? This article examines the territorial disputes between South Korea and Japan over Dokdo, and between Taiwan and Japan over the Senkaku Islands. It sets forth a rhetorical framework of comparison, and it proposes a constructivist perspective in understanding South Korea’s and Taiwan’s legitimation strategies toward Japan from the late 1990s to 2018. This comparative study suggests that the differences between their legitimation strategies can be traced to their different colonial experiences with Japan.

The first results of isotopic (U-Pb, ID-TIMS) dating of individual zircon grains from dolerite dikes of the Eastern zone of the Urals

LITOSFERA ◽  
2020 ◽  
Vol 20 (2) ◽  
pp. 224-230
Author(s):  
V. N. Smirnov ◽  
K. S. Ivanov ◽  
T. V. Bayanova
Keyword(s):  
Isotope Geochemistry ◽  
Early Carboniferous ◽  
Dynamic Mode ◽  
Middle Urals ◽  
Volcanic Complex ◽  
The Urals ◽  
Electron Multiplier ◽  
The Middle Urals ◽  
Eastern Zone ◽  
First Results

Research subject. The article presents the results of dating two dolerite dikes differing in geochemical features from a section along the Iset river in the area of Smolinskoe settlement (the Eastern zone of the Middle Urals). Materials and methods. The dating was performed by an U-Pb ID-TIMS technique for single zircon grains using an artificial 205Pb/235U tracer in the laboratory of geochronology and isotope geochemistry of the Geological Institute of the Kola Science Centre of the Russian Academy of Sciences. The lead isotopic composition and uranium and lead concentrations were measured using a Finnigan-MAT (RPQ) seven-channel mass spectrometer in dynamic mode using a secondary electron multiplier and RPQ quadrupole in ion counting mode. Results. The dikes were dated 330 ± 3 Ma and 240 ± 2 Ma. Conclusions. The research results indicate different ages of dolerite dikes developed within the Eastern zone of the Middle Urals. The oldest of the two established age levels corresponds to the Early Carboniferous era. This fact, along with the proximity of the dolerites to the petrochemical features of the basaltoids of the Early Carboniferous Beklenischevsky volcanic complex, allows these bodies to be considered as hypabyssal comagmates of these volcanics. The youngest obtained age level – Triassic – indicates that the introduction of some dolerite dikes was associated with the final phases of the trapp formation developed rarely within the eastern outskirts of the Urals and widely further east in the foundation (pre-Jurassic basement) of the West-Siberian Plate.

Dissymmetry in form of the Urals type diamond

2018 ◽  
Vol 147 (6) ◽  
pp. 113-132
Author(s):  
Rakin V.I. ◽  
◽  
Pomazansky B.S. ◽  
Kovalchuk O.E. ◽  
◽  
...  
Keyword(s):  
The Urals

Sedelnikovaea baicalensis (Lecanoraceae) — new lichen genus and species for Europe

2018 ◽  
Vol 52 (2) ◽  
pp. 407-416
Author(s):  
T. V. Makryi
Keyword(s):  
Central Asia ◽  
Lichen Species ◽  
Significant Part ◽  
The Urals ◽  
Southern Siberia ◽  
Central Asian ◽  
Northeastern Siberia ◽  
Mountain Belts ◽  
First Time ◽  
Vast Range

Sedelnikovaea baicalensis, the Siberian-Central Asian lichen species, is recorded for the first time for Europe. Based on all the known localities, including those first-time reported from Baikal Siberia, the peculiarities of the ecology and distribution of this species are discussed, the map of its distribution is provided. It is concluded that the species was erroneously considered earlier as a Central Asian endemic. The center of the present range of this lichen is the steppes of Southern Siberia and Mongolia. Assumptions are made that S. baicalensis is relatively young (Paleogene-Neogene) species otherwise it would have a vast range extending beyond Asia, and also that the Yakut locations of this species indicate that in the Pleistocene its range was wider and covered a significant part of the Northeastern Siberia but later underwent regression. Based on the fact that in the mountains of Central Asia the species is found only in the upper mountain belts, it is proposed to characterize it as «cryo-arid xerophyte» in contrast to «arid xerophytes». A conclusion is made that the presence of extensive disjunctions of S. baicalensis range between the Southern Pre-Urals and the Altai-Sayan Mountains or the Mountains of Central Asia is unlikely; the lichen is most likely to occur in the Urals and most of Kazakhstan.

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